The Source Crater of Martian Shergottite Meteorites
Absolute ages for planetary surfaces are often inferred by crater densities and only indirectly constrained by the ages of meteorites. We show that the
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 2014-03, Vol.343 (6177), p.1343-1346 |
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Hauptverfasser: | , , |
Format: | Artikel |
Sprache: | eng |
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Online-Zugang: | Volltext |
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Zusammenfassung: | Absolute ages for planetary surfaces are often inferred by crater densities and only indirectly constrained by the ages of meteorites. We show that the |
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ISSN: | 0036-8075 1095-9203 |
DOI: | 10.1126/science.1247282 |